![]() Rocky deserts offer the perfect combination. Therefore, the hottest LSTs are likely to occur where the skies are clear, the soil is dry, the winds are light, and the ground absorbs most light and reflects little&mdsash that is, has a low albedo. On the other hand, land skin temperatures reflect the direct heating of a parcel of ground by radiation from the sun, the atmosphere, and other heat flows. Moisture also regulates how much heat can be stored in the air. Air temperatures are moderated by circulation-both the rising and sinking of air masses into the atmosphere, and the horizontal movement of winds across the landscape. The difference between air temperatures and land skin temperatures is a result of how heat is transferred and transmitted. And in 2008, the yearly maximum temperature of 66.8☌ (152.2☏) was recorded in the Turpan Basin of the Taklimakan Desert in China. In 2003, the satellites recorded a temperature of 69.3☌ (156.7☏)-the second highest in the seven-year analysis-in the badlands of Queensland, Australia. The single highest LST recorded in any year occurred there in 2005, when MODIS recorded 70.7☌ (159.3☏)-more than 12☌ (22☏) warmer than the official world record air temperature from Libya.īut the Lut Desert was not the hottest every year. In five of the seven years-2004, 2005, 2006, 2007, and 2009-the highest surface temperature on Earth was found in the Lut Desert of Iran. These land skin temperature measurements have helped scientists from the University of Montana pinpoint the hottest places in the world. Since the two MODIS instruments scan the entire surface each day, they provide a complete picture of earthly temperatures and fill in the gaps between the world’s weather stations-particularly in extreme environments where temperatures are simply not measured. The MODIS instrument has 36 different spectral bands (groups of wavelengths), including some that detect thermal radiance, or the amount of infrared energy emitted by the land surface. ![]() Below the image, click on the links to view an animation showing the different maximum temperatures for each year. The map above shows global maximum land surface (or skin) temperatures from 2003 to 2009, as measured by the Moderate Resolution Imaging Spectroradiometer (MODIS) onboard NASA’s Terra and Aqua satellites. The air temperature a meter above the ground was 42.5☌ (108.5☏). In the midday sun, the temperature at 0.4 centimeters below the soil surface was 71.5☌ (160.7☏). ![]() Scientists first measured that difference in June 1915 near Tucson, Arizona. The surface beneath your feet feels much hotter than the air around your head. LSTs are often significantly hotter than air temperatures, and if you’ve ever walked barefoot across hot sand or pavement on a summer day, you know the difference. Scientists are also interested in land “skin” temperature (LST), a measure of direct heating of the land surface, where the Sun’s rays are absorbed and re-emitted. However, it cannot be measured in the shade of a building, mountain, or tree.īut air temperatures are just one way to think about how the Earth is warmed by the Sun and the atmosphere. The air temperatures reported by your local meteorologist are measured by a thermometer situated 1.2 to 2 meters off the ground and shielded from direct sun. National Weather Service, and other scientific institutions have established some very specific guidelines for how to do it. The traditional way to measure temperatures on Earth is with a thermometer, and the World Meteorological Organization, the U.S.
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